A comparison of foraminiferal and diatom-based transfer function estimates of coseismic subsidence during the 1700 CE earthquake along the Oregon and California coasts
Tina Dura1, Eileen Hemphill-Haley2, Niamh Cahill3, Harvey M Kelsey2, Andrea Hawkes4, Diego Melgar5, David Bruce1, Isabel Hong6, Simon Engelhart7, Robert Carleton Witter8, Jason Scott Padgett9, Alan R Nelson10, Yvonne Milker11 and Benjamin Peter Horton12, (1)Virginia Polytechnic Institute and State University, Geosciences, Blacksburg, United States, (2)Humboldt State University, Arcata, United States, (3)University of Massachusetts Amherst, Department of Biostatistics and Epidemiology, Amherst, United States, (4)University of North Carolina at Wilmington, Earth and Ocean Sciences, Wilmington, NC, United States, (5)University of Oregon, Department of Earth Sciences, Eugene, OR, United States, (6)Central Washington University, Ellensburg, WA, United States, (7)University of Durham, Department of Geography, Durham, United Kingdom, (8)USGS Alaska Science Center, Anchorage, AK, United States, (9)University of Rhode Island, Department of Geosciences, Narragansett, RI, United States, (10)US Geological Survey, Denver, CO, United States, (11)University of Hamburg, Hamburg, Germany, (12)Rutgers University New Brunswick, Marine and Coastal Sciences, New Brunswick, United States
